| mhorn | Дата: Wednesday, 21.10.2009, 22:59 | Сообщение # 1 |
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| Branski P. (2009) Influence of palaeoclimate and the greenhouse effect on Hettangian clay mineral assemblages (Holy Cross Mts. area, Polish Basin) // Geol. Quart., 53 (3): 363–368. Warszawa.
pdf: http://www.pgi.gov.pl/images/stories/G_Q/53_3/branski.pdf
Hettangian clay mineral assemblages from the Holy Cross Mts. margin (south eastern part of the epicontinental Polish Basin) were mostly controlled by climatic conditions and weathering regime. Hettangian claystones and mudstones were deposited in continental and marine-margin palaeoenvironments in a warm climate, mostly with year-round humidity. The pronounced, long-term greenhouse conditions intensified chemical weathering in the hinterland. Reworking and redeposition of ancient sediments caused by tectonics and/or by sea-level changes and early diagenesis may have modified the clay mineral content in the earliest Hettangian. Burial diagenesis and telodiagenesis changed the clay mineral composition only locally.
Middle Jurassic - Lower Cretaceous ammonites & aptychi
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